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M. R. Barchi on Muck Rack

M. R. Barchi

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Rock and fault rheology explain differences between on fault and distributed seismicity - Nature Communications

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By C. Collettini, F. Trippetta, M. R. Barchi, N. De Paola
| Nature Verified
The frequency-magnitude distribution of earthquakes is usually modelled with an exponential function, called Gutenberg-Richter law, written as: ln N(M) = a–bM, where N(M) represents the number of events with magnitude larger than M, a is the productivity and b controls the relative rate of small and large earthquakes. Estimating the b-value appears trivial in theory but not in practice41,58.
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